
gemstone
Tumbled agate or chalcedony
Microcrystalline quartz (SiO₂), likely gray-brown agate/chalcedony
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; translucent gray-brown body with subtle curved banding, waxy to vitreous luster, and no visible cleavage. The smoothly rounded shape indicates tumbling and polishing; exact identification is limited by the photograph.
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Physical properties
Hardness 6.5–7 Mohs; translucent gray-brown body with subtle curved banding, waxy to vitreous luster, and no visible cleavage. The smoothly rounded shape indicates tumbling and polishing; exact identification is limited by the photograph.
Formation & geological history
Agate forms when silica-rich groundwater fills cavities in volcanic rock, depositing layered chalcedony over geologic time, commonly during the Cenozoic or older volcanic episodes. It is later cut and mechanically tumbled for decoration.
Uses & applications
Used for cabochons, beads, carvings, paperweights, and inexpensive jewelry; polished pieces are popular educational and collecting specimens.
Geological facts
Agate is a variety of chalcedony distinguished by cryptocrystalline quartz and commonly concentric or irregular color bands. Its color may be natural or enhanced by dye or surface coating.
Field identification & locations
Look for waxy luster, translucency at thin edges, curved internal banding, and resistance to scratching by steel; a glassy appearance or bubbles would suggest imitation glass. Common sources include Brazil, Uruguay, Mexico, India, and the United States.
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